茶叶科学技术
茶葉科學技術
다협과학기술
TEA SCIENCE AND TECHNOLOGY
2014年
3期
13-19
,共7页
王峰%陈玉真%尤志明%吴志丹%江福英%陈芝芝
王峰%陳玉真%尤誌明%吳誌丹%江福英%陳芝芝
왕봉%진옥진%우지명%오지단%강복영%진지지
土壤类型%茶园%团聚体有机碳
土壤類型%茶園%糰聚體有機碳
토양류형%다완%단취체유궤탄
tea plantation%soil aggregate%organic carbon
采用野外调查和室内分析相结合的方法,研究福建省武夷山市5种不同类型茶园土壤(黄壤、红壤、潮砂土、高山草甸土、紫色土)团聚体有机碳分布特征。结果表明:5种类型茶园土壤各粒级团聚体有机碳含量均随土壤层次的加深呈现降低的趋势;2个土层中,5种类型茶园土壤团聚体有机碳含量均以>5 mm粒径最高,随着土壤团聚体粒径的增加,团聚体有机碳增加;黄壤、高山草甸土和紫色土茶园均以>5 mm粒径团聚体有机碳储量和贡献率最高,而潮砂土则以<0.25 mm粒径最高;土壤有机碳含量与各粒径团聚体有机碳含量呈极显著正相关(相关系数为0.95~0.98)。
採用野外調查和室內分析相結閤的方法,研究福建省武夷山市5種不同類型茶園土壤(黃壤、紅壤、潮砂土、高山草甸土、紫色土)糰聚體有機碳分佈特徵。結果錶明:5種類型茶園土壤各粒級糰聚體有機碳含量均隨土壤層次的加深呈現降低的趨勢;2箇土層中,5種類型茶園土壤糰聚體有機碳含量均以>5 mm粒徑最高,隨著土壤糰聚體粒徑的增加,糰聚體有機碳增加;黃壤、高山草甸土和紫色土茶園均以>5 mm粒徑糰聚體有機碳儲量和貢獻率最高,而潮砂土則以<0.25 mm粒徑最高;土壤有機碳含量與各粒徑糰聚體有機碳含量呈極顯著正相關(相關繫數為0.95~0.98)。
채용야외조사화실내분석상결합적방법,연구복건성무이산시5충불동류형다완토양(황양、홍양、조사토、고산초전토、자색토)단취체유궤탄분포특정。결과표명:5충류형다완토양각립급단취체유궤탄함량균수토양층차적가심정현강저적추세;2개토층중,5충류형다완토양단취체유궤탄함량균이>5 mm립경최고,수착토양단취체립경적증가,단취체유궤탄증가;황양、고산초전토화자색토다완균이>5 mm립경단취체유궤탄저량화공헌솔최고,이조사토칙이<0.25 mm립경최고;토양유궤탄함량여각립경단취체유궤탄함량정겁현저정상관(상관계수위0.95~0.98)。
A combined method of field investigation and laboratory analysis was conducted to study the distribution features of organic carbon in soil aggregates from different tea plantations (yellow soil, red earth, moisture sandy soil, alpine meadow soil and purple soil) in Wuyishan City. The results showed that a depth-dependent manner was found in 5 soil aggregates with the content of organic carbon decreasing higher at 0~20 cm and less at 20~40 cm. There was a positive correlation between the contents of organic carbon and particle sizes of soil aggregate and most was exhibited at >5 mm in 5 tea plantation soils. The storage and distribution ratios of organic carbon were the highest while particle size of soil aggregates>5 mm in yellow soil, alpine meadow soil and purple soil, and<0.25 mm in moisture sandy soil, respectively. From the results, the contents of organic carbon in soil have an extremely significant positive correlation with its aggregates.